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Richard L. Reynolds Joseph G. Rosenbaum Josh Rapp Michael W. Kerwin J. Platt Bradbury Steven Colman David Adam 《Journal of Paleolimnology》2004,31(2):217-233
Petrological and textural properties of lacustrine sediments from Upper Klamath Lake, Oregon, reflect changing input volumes of glacial flour and thus reveal a detailed glacial history for the southern Cascade Range between about 37 and 15 ka. Magnetic properties vary as a result of mixing different amounts of the highly magnetic, glacially generated detritus with less magnetic, more weathered detritus derived from unglaciated parts of the large catchment. Evidence that the magnetic properties record glacial flour input is based mainly on the strong correlation between bulk sediment particle size and parameters that measure the magnetite content and magnetic mineral freshness. High magnetization corresponds to relatively fine particle size and lower magnetization to coarser particle size. This relation is not found in the Buck Lake core in a nearby, unglaciated catchment. Angular silt-sized volcanic rock fragments containing unaltered magnetite dominate the magnetic fraction in the late Pleistocene sediments but are absent in younger, low magnetization sediments. The finer grained, highly magnetic sediments contain high proportions of planktic diatoms indicative of cold, oligotrophic limnic conditions. Sediment with lower magnetite content contains populations of diatoms indicative of warmer, eutrophic limnic conditions. During the latter part of oxygen isotope stage 3 (about 37–25 ka), the magnetic properties record millennial-scale variations in glacial-flour content. The input of glacial flour was uniformly high during the Last Glacial Maximum, between about 21 and 16 ka. At about 16 ka, magnetite input, both absolute and relative to hematite, decreased abruptly, reflecting a rapid decline in glacially derived detritus. The decrease in magnetite transport into the lake preceded declines in pollen from both grass and sagebrush. A more gradual decrease in heavy mineral content over this interval records sediment starvation with the growth of marshes at the margins of the lake and dilution of detrital material by biogenic silica and other organic matter. 相似文献
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芒果嫁接成活气象条件及生产管理措施 总被引：3，自引：0，他引：3
利用芒果嫁接成活率多年分期物候观测以及同期的气象观测实况资料进行统计分析。结果表明,芒果嫁接成活率与嫁接后的接口愈合期气温成显著正相关,与光照、降水量、空气相对湿度相关不明显。建立了芒果嫁接成活率与嫁接后6天平均气温、最高气温回归方程,影响芒果嫁接成活的主要气象要素是日均温。个例分析表明芒果嫁接成活关键期即嫁接穗生理脆弱的接口愈合期,气温偏低或异常高温天气对芒果嫁接成活不利影响极大。讨论了依气象条件提高嫁接成活率注意事项,提出了相应的生产管理措施。 相似文献
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阴离子交换色谱-电感耦合等离子体质谱联用技术用于面粉中溴形态分析 总被引：1，自引：0，他引：1
建立的阴离子交换色谱-电感耦合等离子体质谱联用技术用于测量面粉中的痕量 BrO3-及Br-。使用DIONEX CarBoPac PA-100(4 mm×250 mm,i．d．)色谱柱,在流速1 mL／min 及5 mmol／L NH4NO3淋洗液下分离BrO3-和Br-。该方法在100μL进样量下BrO3-的检出限为 0．0027 μmoL／L(0．22μg／L),Br-为0．0067 μmoL／L(0．54μg／L)。对市场上部分面粉类样品的分析结果表明,所选面粉只有一种检出有BrO3-,其他样品中的BrO3-均低于检出限。方法的回收率可达到98％-109％。 相似文献
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根据芒果生产与气象条件的关系 ,分析确定了百色地区芒果种植的农业气候区划指标 ,进行了区划指标的小网格点推算 ;采用 GIS技术对百色地区芒果种植区进行农业气候区划 ,划分适宜、次适宜和不适宜种植区 ,提出趋利避害合理发展芒果生产的措施和建议 ,为农业结构调整及芒果的合理布局提供科学依据 相似文献
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样品用硝酸-高氯酸混合酸消解，考察了氢化物发生-原子荧光光谱法测定面粉中微量砷的实验条件，包括混合酸和还原剂硼氢化钾的用量。方法测定砷的线性范围为0．0—30．0μg／L，仪器的检出限为0．26μg／L，加标回收率为94．0％-104．0％，方法的精密度（RSD，n=11）为1．16％。方法操作简便、快速、灵敏度高。 相似文献
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海南省芒果寒害气象指数保险费率厘定及保险合同设计研究 总被引：1，自引：0，他引：1
寒害严重影响和制约海南芒果种植业的发展,芒果寒害气象指数保险费率的厘定及其合同设计对于转移灾害风险、减少农民损失、促进海南经济发展具有重大意义。利用海南省18个市(县)1990-2010年的芒果产量数据和1961-2010年的气象数据,基于极值理论构建产量风险分布模型,厘定了各市(县)的纯保险费率及其空间分布。结果表明:纯保险费率高值区主要分布在中部山区的五指山、琼中和白沙,以及北部的澄迈,其中白沙最高,这些地区芒果寒害风险较高,且种植技术或防灾减灾能力较差,建议采用高免赔额费率;纯保险费率低值区主要分布在南部和东部,其中南部三亚和陵水无寒害,其他市(县)寒害风险较低,建议实行低免赔额费率。同时,设计了基于不同免赔额的保险产品及合同,可为海南建立和完善芒果政策性农业保险方案提供技术支撑。 相似文献
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【目的】研究添加芒果粉对真空油炸面包虾裹浆特性及其品质的影响。【方法】以小麦粉和大豆分离蛋白的裹浆作为对照,研究芒果粉替代部分小麦粉和大豆分离蛋白的裹浆流变学特性;以裹涂率、油脂含量、水分含量、色泽及质构特性为考察指标,研究芒果粉替代部分小麦粉和大豆分离蛋白的裹浆对真空油炸面包虾品质的影响;以最佳芒果粉添加量的真空油炸面包虾为研究对象,测定外裹层黄酮物质含量,并采用羟自由基和DPPH自由基体系对产品外裹层黄酮物质的抗氧化性进行分析。【结果】所有配方的裹浆均表现为触变性,呈现剪切稀化特性,具有假塑性流体特征,并符合幂率流体,芒果粉可显著提升裹浆的黏度;芒果粉可显著增大面包虾裹涂率,改善产品质构和色泽特性,降低产品油脂含量并提升其水分含量(P <0.05)。当芒果粉添加量从10%增加到30%时,面包虾产品油脂质量分数从24.84%降低到20.58%,产品的脆性和色泽中的亮度值(L*)、黄度值(b*)均得到了显著提升(P <0.05)。当小麦粉质量分数66%、大豆分离蛋白质量分数4%、芒果粉质量分数30%时,真空油炸面包虾产品的各项品质最佳;真空油炸面包虾产品外裹层黄酮物质质量分数为(46.75±2.87)mg/100g,其对羟自由基和DPPH自由基的清除效果方面都均强于维生素C。【结论】芒果粉可提升裹浆黏度,改善真空油炸面包虾产品品质,其外裹层较强的抗氧化性对于真空油炸裹涂制品延长货架期具有一定积极作用。 相似文献
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Tidal observations on the West Coast,South Island,New Zealand 总被引：1，自引：1，他引：0
R. A. Heath 《新西兰海洋与淡水研究杂志》2013,47(2):251-261
Harmonic tidal constants, calculated from sea surface elevation observations at Jackson Bay on the West Coast of the South Island, are consistent with available semi‐diurnal and diurnal tidal phase distributions. Current observations taken over a 111 day period at mid‐depth in 1505 m of water on the southern flank of the Challenger Plateau and over a 240 day period in 1430 m of water on the South Island western coast continental slope, are subject to tidal analysis. At both sites there is a component of energy flux directed across the isobaths and only at the northern site for the M2 tide is the phase consistent with a dominant progressive barotropic tide. The successive 30 day harmonic constants at the southern continental slope site exhibit a trend in the M2 tidal ellipse speed and ellipticity suggesting the presence of a regular internal tide. Superposition of ‘internal tidal’ and barotropic tidal flows, as prescribed from progressive‐ and standing‐wave elevations, to fit the observations indicates that the ‘internal tide’ is probably associated with the first baroclinic mode. At the current‐meter depths the speeds of the ‘internal tide’ for the M2 tide are about the same as the barotropic speeds, whereas, the S2 ‘internal tide’ speeds are larger than those of the barotropic tide. The consistency of the trend in ellipse parameters lends support to the theoretical progressive trapped barotropic tidal flows being a good approximation to the actual barotropic tide. Some support for the hypothesis that the S2 tide on the West Coast of New Zealand has a substantial standing wave contribution is given by the northern observations, where the ratio of the S2: M2 internal tidal ellipse current amplitudes are substantially larger than the ratio of the elevations, the internal tide being generated by across‐isobath flows. 相似文献
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正20140958 Mei Huicheng(No.915GeologicalBrigade,Jiangxi Bureau of Geology and Mineral Resources,Nanchang 330002,China);Li Zhongshe Geological Features and Causes of the Huihuang Geotherm in Xiushui,Jiangxi Province(Journal of Geological Hazards and 相似文献